{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1363670318897348992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/nhess-12-1017-2012"}},{"identifier":{"@type":"URI","@value":"https://nhess.copernicus.org/articles/12/1017/2012/nhess-12-1017-2012.pdf"}}],"dc:title":[{"@value":"Modeling propagation and inundation of the 11 March 2011 Tohoku tsunami"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. On 11 March 2011 the Tohoku tsunami devastated the east coast of Japan, claiming thousands of casualties and destroying coastal settlements and infrastructure. In this paper tsunami generation, propagation, and inundation are modeled to hindcast the event. Earthquake source models with heterogeneous slips are developed in order to match tsunami observations, including a best fit initial sea surface elevation with water levels up to 8 m. Tsunami simulations were compared to buoys in the Pacific, showing good agreement. In the far field the frequency dispersion provided a significant reduction even for the leading wave. Furthermore, inundation simulations were performed for ten different study areas. The results compared well with run-up measurements available and trim lines derived from satellite images, but with some overestimation of the modeled surface elevation in the northern part of the Sanriku coast. For inundation modeling this work aimed at using freely available, medium-resolution data for topography, bottom friction, and bathymetry, which are easily accessible in the framework of a rapid assessment. Although these data come along with some inaccuracies, the results of the tsunami simulations suggest that their use is feasible for application in rapid tsunami hazard assessments. A heterogeneous source model is essential to simulate the observed distribution of the run-up correctly, though.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380849946839550729","@type":"Researcher","foaf:name":[{"@value":"F. Løvholt"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318897348994","@type":"Researcher","foaf:name":[{"@value":"G. Kaiser"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318897348996","@type":"Researcher","foaf:name":[{"@value":"S. Glimsdal"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318897348992","@type":"Researcher","foaf:name":[{"@value":"L. Scheele"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318897348997","@type":"Researcher","foaf:name":[{"@value":"C. B. Harbitz"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318897348995","@type":"Researcher","foaf:name":[{"@value":"G. Pedersen"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"16849981"}],"prism:publicationName":[{"@value":"Natural Hazards and Earth System Sciences"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2012-04-16","prism:volume":"12","prism:number":"4","prism:startingPage":"1017","prism:endingPage":"1028"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/3.0/"],"url":[{"@id":"https://nhess.copernicus.org/articles/12/1017/2012/nhess-12-1017-2012.pdf"}],"createdAt":"2012-04-16","modifiedAt":"2022-01-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215254657024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Parallel Implementation of Dispersive Tsunami Wave Modeling with a Nesting Algorithm for the 2011 Tohoku Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166056219008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Accurate numerical simulation of the far-field tsunami caused by the 2011 Tohoku earthquake, including the effects of Boussinesq dispersion, seawater density stratification, elastic loading, and gravitational potential change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168540501632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Risk Assessment and Design of Prevention Structures for Enhanced Tsunami Disaster Resilience (RAPSODI)/Euro-Japan Collaboration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593678873728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid assessment of tsunami source impacts on low-lying coastal areas using offshore wave superposition and static sweep of onshore terrain"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205357457664","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analysis of tsunami evacuation caused by the Great East Japan Earthquake:A case study of Ibaraki Prefecture"},{"@language":"ja","@value":"津波発生時の避難行動解析：2011 年東北地方太平洋沖地震における茨城県での津波避難"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266977822464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frequency-dependent amplification of the Sanriku tsunamis in Ryori Bay"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/nhess-12-1017-2012"},{"@type":"CROSSREF","@value":"10.1007/s00024-015-1049-2_references_DOI_8Yha5Wp0VBv5PrKMGdft89IkkCe"},{"@type":"CROSSREF","@value":"10.5610/jaee.13.4_19_references_DOI_8Yha5Wp0VBv5PrKMGdft89IkkCe"},{"@type":"CROSSREF","@value":"10.1142/s057856341640012x_references_DOI_8Yha5Wp0VBv5PrKMGdft89IkkCe"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1128-1_references_DOI_8Yha5Wp0VBv5PrKMGdft89IkkCe"},{"@type":"CROSSREF","@value":"10.1080/21664250.2021.2005364_references_DOI_8Yha5Wp0VBv5PrKMGdft89IkkCe"},{"@type":"CROSSREF","@value":"10.1016/j.ocemod.2017.01.002_references_DOI_8Yha5Wp0VBv5PrKMGdft89IkkCe"}]}